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inel pigment CaFe O obtained by the ecu

by unknown authors
"... roup shingt 3; acc phys ccom flecta quality, there are important factors—synthesis method deter- ly by glaze material during its melting, in other words, the 004)Color is an optical property that takes to countless applications. For ceramic tiles, pigments give a stable coloration to a glaze, throug ..."
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throughout the matrix [4,5]. After synthesis, CaFe2O4 physical and chemical behavior was studied, verifying its stability as pigment under industrial conditions.also physical and chemical properties.mines not only stoichiometric and morphologic control but pigment should be insoluble in glazes (substrate) [3

High pressure synthesis and electrochemical properties of CaFe2O4-type LiMn2O4

by unknown authors
"... Since their commercialization in the 1990s, lithium-ion batteries have been widely used as electric power supply of portable electronic devices [1].Lithiated transition metal oxides such as LiCoO2 and spinel-type ..."
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Since their commercialization in the 1990s, lithium-ion batteries have been widely used as electric power supply of portable electronic devices [1].Lithiated transition metal oxides such as LiCoO2 and spinel-type

Mössbauer Study of Two Discernable Fe Sites in CaFe 2 O 4

by Sunghyun Yoon
"... Structural and magnetic properties of polycrystalline CaFe ..."
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Structural and magnetic properties of polycrystalline CaFe

Crystal-chemical characterization of NaA1SiO4 with the CaFe204 structure

by Hirohisa Yamada, Yoshito Matsui, Eiji Ito
"... ABSTRACT. A high-pressure modification of NaA1SiO, with the calcium ferrite structure was synthesized at pressures higher than 24 GPa using a double-stage split-sphere type high-pressure apparatus. The unit cell dimensions are: a=10.1546(8), b=8.6642(8), c= 2.7385(4) A, and V = 240.93(3) A a with th ..."
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ABSTRACT. A high-pressure modification of NaA1SiO, with the calcium ferrite structure was synthesized at pressures higher than 24 GPa using a double-stage split-sphere type high-pressure apparatus. The unit cell dimensions are: a=10.1546(8), b=8.6642(8), c= 2.7385(4) A, and V = 240.93(3) A a

Optical Floating Zone Growth of Single Crystal r-Fe2O3 from a CaFe4O7-Based Solvent

by Courtney H. Lanier, Peter C. Stair, Laurence D. Marks , 2004
"... ABSTRACT: Large single crystals ( … 5 L 33 mm) of hematite (R-Fe2O3) have been grown using a CaFe4O7-based solvent and 8 bar of oxygen in a four-mirror optical floating zone furnace in the traveling solvent zone configuration. The crystals grow along the [001] direction, are of excellent quality, a ..."
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ABSTRACT: Large single crystals ( … 5 L 33 mm) of hematite (R-Fe2O3) have been grown using a CaFe4O7-based solvent and 8 bar of oxygen in a four-mirror optical floating zone furnace in the traveling solvent zone configuration. The crystals grow along the [001] direction, are of excellent quality

Competitive Reaction During Decomposition of Hexachlorobenzene Over Ultrafine Ca–Fe Composite Oxide Catalyst

by Minghui Zheng
"... Abstract The decomposition of hexachlorobenzene (HCB) has been investigated over ultrafine Ca–Fe com-posite oxide catalyst (Ca/Fe atomic ratio was 3.4), CaO and a-Fe2O3 by using in situ diffuse reflectance infrared Fourier transform spectroscopy (DRIFTS). Adsorption experiments on the surface of oxi ..."
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Abstract The decomposition of hexachlorobenzene (HCB) has been investigated over ultrafine Ca–Fe com-posite oxide catalyst (Ca/Fe atomic ratio was 3.4), CaO and a-Fe2O3 by using in situ diffuse reflectance infrared Fourier transform spectroscopy (DRIFTS). Adsorption experiments on the surface

Sveinbergeite, Ca(Fe2+6 Fe 3+)Ti2(Si4O12)2O2(OH)5(H2O)4, a new astrophyllite-group mineral from the Larvik Plutonic Complex, Oslo Region, Norway: description and crystal structure

by A. P. Khomyakov, E. Sokolova, Y. Abdu, F. C. Hawthorne , 2011
"... Sveinbergeite, Ca(Fe2+6 Fe 3+)Ti2(Si4O12)2O2(OH)5(H2O)4, is a new astrophyllite-group mineral discovered in a syenite pegmatite at Buer on the Vesterøya peninsula, Sandefjord, Oslo Region, Norway. The mineral occurs in pegmatite cavities as 0.010.05 mm thick lamellar (0.20.56510 mm) crystals forming ..."
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Sveinbergeite, Ca(Fe2+6 Fe 3+)Ti2(Si4O12)2O2(OH)5(H2O)4, is a new astrophyllite-group mineral discovered in a syenite pegmatite at Buer on the Vesterøya peninsula, Sandefjord, Oslo Region, Norway. The mineral occurs in pegmatite cavities as 0.010.05 mm thick lamellar (0.20.56510 mm) crystals

Lattice dynamics of ZnAl 2 O 4 and ZnGa 2 O 4 under high pressure

by S López-Moreno , P Rodríguez-Hernández , A Muñoz , A H Romero , F J Manjón , D Errandonea , E Rusu , V V Ursaki , 2011
"... In this work we present a first-principles density functional study of the vibrational properties of ZnAl2O4 and ZnGa2O4 as function of hydrostatic pressure. Based on our previous structural characterization of these two compounds under pressure, herewith, we report the pressure dependence on both ..."
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systems of the vibrational modes for the cubic spinel structure, for the CaFe2O4-type structure (Pnma) in ZnAl2O4 and for marokite (Pbcm) ZnGa2O4. Additionally we report a second order phase transition in ZnGa2O4 from the marokite towards the CaTi2O4-type structure (Cmcm), for which we also calculate

Competition/Coexisitence of Magnetism and Superconductivity in Iron Pnictides Probed by Muon Spin Rotation

by Soshi Takeshita, Ryosuke Kadono , 812
"... Abstract. The presence of macroscopic phase separation into superconducting and magnetic phases in LaFeAsO1−xFx and CaFe1−xCoxAsF is demonstrated by muon spin rotation (µSR) measurement across their phase boundaries (x = 0.06 for LaFeAsO1−xFx and x = 0.075–0.15 for CaFe1−xCoxAsF). In LaFeAsO0.94F0.0 ..."
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, an assessment is made on the anisotropy of order parameter in the superconducting state of LaFeAsO1−xFx, CaFe1−xCoxAsF, and Ba1−xKxFe2As2 (x = 0.4) based on the temperature dependence of superfluid density [ns(T)] measured by µSR. The gap parameter, 2∆/kBTc, determined from ns(T) exhibits a tendency that hole

unknown title

by unknown authors
"... Ternary rare earth oxides EuLn2O4 (Ln = Gd, Dy-Lu) were prepared. They crystallized in an orthorhombic CaFe2O4-type structure with space group Pnma. 151Eu Mössbauer spectroscopic measurements show that the Eu ions are in the divalent state. All these compounds show an antiferromagnetic transition at ..."
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Ternary rare earth oxides EuLn2O4 (Ln = Gd, Dy-Lu) were prepared. They crystallized in an orthorhombic CaFe2O4-type structure with space group Pnma. 151Eu Mössbauer spectroscopic measurements show that the Eu ions are in the divalent state. All these compounds show an antiferromagnetic transition
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